CAJ | 학술논문

保定西部太行山区广泛发育强透水岩层、低阻岩脉和富水构造。在该地区寻找构造裂隙水时，关键在于准确区分低阻岩脉(体)与富水断层。利用水文地质调查和物探勘查相结合的方法，通过对比分析低阻岩脉与富水断层的电性差异，成功实施了一眼构造裂隙水勘查示范井。取得了岩脉区寻找构造裂隙水的有效方法，解决了当地多年缺水问题。
보정서부태행산구엄범발육강투수암층、저조암맥화부수구조。재해지구심조구조렬극수시，관건재우준학구분저조암맥(체)여부수단층。이용수문지질조사화물탐감사상결합적방법，통과대비분석저조암맥여부수단층적전성차이，성공실시료일안구조렬극수감사시범정。취득료암맥구심조구조렬극수적유효방법，해결료당지다년결수문제。
A large number of permeable rocks, low-resistance veins, and water-rich structures occur in the Taihang mountains ar-ea of western Baoding. To explore the structural fissure water in this area, the key is to howto distinguish the low-resistance veins from water-rich faultaccurately. Based on the hydrogeological conditions survey and geophysical exploration, a demonstra-tion well of structural fissure water was successfully implemented through the comparative analysis of the electrical difference between low-resistance veins and water-rich fault. Therefore, the methods to find structural fissure water in the vein developing area was obtained, which solved the water shortage problem in this area.